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Heterogeneity and Controlling Factors of Oxfordian Stage Carbonate Reservoir of Odjarly Gas Field, Amu Darya Basin

机译:Odjarly气田氧代德碳酸盐储层的异质性和控制因素,AMU Darya盆地

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Based on core observation and thin section authentication, the control factors of Oxfordian Stage carbonate reservoir of Odjarly Gas field of Amu Darya Basin were discussed by comprehensive utilization of geological, drilling, seismic data etc. It was concluded that the carbonate reservoir developed mainly in grain limestone, oolitic limestone and conglomeratic bioclast limestone. Lithology controlled directly the porosity of reservoir, and the porosity of grain limestone was the highest. The analysis showed that the carbonate reservoir quality of the Oja-21 was under the control of the sedimentary microfacies. The oolite beach and microfacies of bioherm phase were the favorable to develop. The physical property of oolite beach was optimal, and it was the most favorable sedimentary microfacies of reservoir development. It concluded also that the heterogeneity of core section of carbonate reservoir of Oja - 21 was mainly controlled by lithology, sedimentary microfacies and diagenesis. As for the core section, the heterogeneity of reservoir could be summarized as interbedded heterogeneity and in-layer heterogeneity.
机译:基于核心观测和薄剖面认证,通过全面利用地质,钻探,地震数据等综合利用了AMU Darya盆地Odjarly气田的氧代气田碳酸钙储层的控制因素。得出结论,碳酸盐储层主要以谷物发育石灰石,鲕粒石灰石和砾岩生物塑料石灰石。岩性控制直接控制储层的孔隙率,谷物石灰石的孔隙度最高。该分析表明,OJA-21的碳酸盐储层质量受到沉积微缩乳的控制。鲕粒海滩和生物阶段的微缩放是有利的。 Oogite Beach的物质性质是最佳的,并且是水库开发中最有利的沉积微缩放。结论,OJA-21碳酸盐储层核心部分的异质性主要由岩性,沉积微缩醛和成岩作用控制。至于芯部分,储层的异质性可以总结为互相异质性和层内异质性。

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